纬向感热输送主要是西风输送。
The zonal sensible heat transfer is mainly by westerly winds.
其经向风分量与纬向风分量同等重要。
The meridional wind component and zonal wind component are same important.
季风环流可以分解为经向环流和纬向环流。
The monsoon circulation can be decomposed into the zonal circulation and the meridional circulation.
这两部分能量分别称作纬向动能和涡旋动能。
These components are known as the zonal kinetic energy and eddy kinetic energy respectively.
下角标Z和E分别表示纬向分量和旋涡分量。
Subscripts Z and E are for zonal and eddy components respectively.
罗纹档是纺类织物纬向方面的主要病疵之一。
深部纬向构造带与北东向构造呈反接复合关系。
The deep latitudinal structural belt shows the transposition relation to the NE trend structures.
在赤道西太平洋暖池,温度的纬向对流有很大的贡献。
The western Pacific warm pool is mainly contributed by zonal temperature advection.
介绍经向为棉纱、纬向为粘胶在棉丝提花织物的前处理工艺。
The pretreatment for jacquard fabric with cotton as warp, rayon as weft is defined.
指出纬向梯度、经向梯度、全梯度矢量的昼夜变化与季节特性。
The latitudinal and longitudinal gradients, their diurnal variations and seasonal characteristics are dealt with.
锦棉弹力闪光交织物经向为锦纶有光丝,纬向为棉氨纶包芯纱。
The nylon-cotton elastic and sparkling fabric is composed of nylon lustrous filament as warp yarn and cotton-polyurethane core-spun yarn as weft yarn.
秦岭纬向构造带不仅在地表发育明显,而且延伸至地幔一定深度。
Qinling latitudinal structural belt is developed very clear on the surface, and extends to a certain depth.
为了使图3不被解释成纬向传播的波的特征,有必要回顾一下前一章所论述的。
Least Fig. 3 be interpreted as the signature of zonally propagating waves, it is worth recalling what is said in the preceding chapter.
全真丝纬向弹力机织物的弹力主要利用强捻纬线的捻度释放来形成。
The elasticity of silk woven fabrics is formed by the twist release of hard twist on weft yarn.
星球级纬向构造体系是控制板块边界和运动的重要的支配力量之一。
The global latitudinal tectonic system is one of the important forces controlling the plate boundary and movement.
该研究为电离层不规则结构纬向漂移速度的测量提供了一种可行的方法。
This research will provide a feasible method for measurement of the ionospheric zonal velocity.
分析了喷气织机纬向停台的原因,介绍了与之相关的调整方法及操作方法。
This paper analyses the reason of filling stop motion of air-jet loom and introduces some methods in adjustment and operation.
ITF的年代际变化是:年代际信号取决于赤道太平洋纬向风应力的变化。
The decadal variation of ITF is that the decadal signal lies in the change of latitude-oriented wind stress in the Equator-Pacific region.
当少台风活动时期,东亚为纬向环流,西南太平洋上赤道西风及ITCZ也弱。
During the inactive period, the circulation of East Asia is essentially zonal and the ITCZ over Southwest Pacific is weak.
当热带东风气流减弱时,低压中心位置偏北,低压强度增强,低压纬向宽度变大;
When the tropical easterly flow decreases, the center position of depression moves northward, the strength of depression increases and the zonal width of depression widens.
发现高空低频扰动动能的高值区与西风急流的纬向非对称性和经向切变关系密切。
The results reveal that the high value areas of the kinetic energy of low-frequency fluctuations in the upper level are closely related with the zonal asymmetry and the meridional shear of westerlies.
模式较好地模拟出了平均海温的经向分布与纬向分布情况,结果与观测基本相符。
The simulated results are consistent with the observation, and the feature of SST's variation as a function of latitude(longitude) is well reproduced.
这种周期振荡现象与赤道平流层的纬向风的准两年周期振荡现象有很好的对应关系。
It is well correspond to zonal wind oscillation on low layer of the stratosphere over Equator.
冬半年大气对赤道东太平洋海温的响应表现为不同于pna的呈纬向分布的模态结构。
The wintertime Northern Hemisphere atmospheric response to SST in EEP is the zonal mode structure which is different from PNA.
分析结果表明,麻竹表型性状的地理变异趋势是以经向变异为主,纬向与垂直变异不明显。
The analysis has shown that the geographical variation trend of phenotypic traits has given priority to longitude, and no obvious variation in latitude and altitude.
本文使用1979—1984年卫星云量资料,分析了赤道太平洋地区平均纬向垂直环流圈。
The mean zonal- vertical circulations in the equatorial Paciric region have been analysed by using 1979- 1984 satellite cloudiness data.
结果发现,中纬度高原的感热加热所造成的经、纬向热力差异是导致亚洲夏季风爆发的原因。
Results show that the longitudinal and latitudinal thermal contrasts caused by the middle latitude Plateau sensible heating trigger the onset of the Asian summer monsoon.
结果表明,近45年西太平洋副高与极涡强度都趋加强,纬向环流趋于加强,经向环流则趋减弱。
It turns out that for the past 45 years or so the western Pacific subtropical highs and polar vortices were intensified, and so were zonal circulations as opposed to meridional ones.
通过建立包含扰动和基流方程组的数值模式,全面讨论了扰动与对称不稳定纬向基流的相互作用。
In a numerical model especially set up in the work that includes disturbance and basic flows, the interactions between disturbances and symmetric instability are discussed comprehensively.
通过建立包含扰动和基流方程组的数值模式,全面讨论了扰动与对称不稳定纬向基流的相互作用。
In a numerical model especially set up in the work that includes disturbance and basic flows, the interactions between disturbances and symmetric instability are discussed comprehensively.
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